Searching for crystal-ice domains in amorphous ices
Fausto Martelli, Nicolas Giovambattista, Salvatore Torquato, Roberto, Car

TL;DR
This study uses molecular dynamics simulations and a local order metric to analyze the structural transformations of water during compression, revealing the presence of ice IV-like domains in high-density amorphous ice and detailing the two-step transition processes.
Contribution
It introduces a sensitive local order metric to distinguish crystalline and amorphous ice structures and demonstrates the structural evolution during phase transitions in water.
Findings
HDA contains ice IV-like domains despite being amorphous.
LDA-to-HDA and I_h-to-HDA transitions are two-step processes.
Higher pressure needed to transform I_h into HDA compared to LDA.
Abstract
We employ classical molecular dynamics simulations to investigate the molecular-level structure of water during the isothermal compression of hexagonal ice (I) and low-density amorphous (LDA) ice at low temperatures. In both cases, the system transforms to high-density amorphous ice (HDA) via a first-order-like phase transition. We employ a sensitive local order metric (LOM) [Martelli et. al., Phys. Rev. B, 97, 064105 (2018)], that can discriminate among different crystalline and non crystalline ice structures and is based on the positions of the oxygen atoms in the first and/or second hydration shell. Our results confirm that LDA and HDA are indeed amorphous, i.e., they lack of polydispersed ice domains. Interestingly, HDA contains a small number of domains that are reminiscent of the unit cell of ice IV, although the hydrogen-bond network (HBN) of these domains differ from the HBN…
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